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Wyszukujesz frazę "quaternary systems" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Calculation of vapour - liquid - liquid - equilibria in quaternary systems
Autorzy:
Wyczesany, A.
Powiązania:
https://bibliotekanauki.pl/articles/185629.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
para-ciecz-ciecz
systemy czwartorzędowe
vapor - liquid - liquid - equilibria
quaternary systems
Opis:
A method of parameters fitting to the experimental vapour - liquid - liquid equilibrium (VLLE) datais presented for the NRTL and the Uniquac equations for six quaternary mixtures. The same equations but with coefficients taken from the simulator Chemcad database were also used for calculation of the VLLE for the same mixtures. The calculated equilibrium temperatures and compositions for all the three phases were compared with the experimental data for these four cases. The investigated models were also applied for calculation of the compositions and temperatures of ternary azeotropes occurring in the considered quaternary mixtures. The computed values were compared with the experimental ones to appreciate the model's accuracy and to confirm whether the model correctly predicts the presence of homo- or heteroazeotrope. The NRTL equation with coefficients fitted to the VLLE data proved to be the most accurate model. For the mixtures containing water, ethanol and two different hydrocarbons this model shows particularly high accuracy. In three cases the mean deviations between the calculated and measured temperatures do not exceed 0.25 K, and for the fourth mixture the difference equals 0.33. Besides, the mean deviations between the calculated and the measured concentrations in the gas and liquid phases, with one exception do not exceed 1 mole %.
Źródło:
Chemical and Process Engineering; 2012, 33, 3; 463-477
0208-6425
2300-1925
Pojawia się w:
Chemical and Process Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrogeological aspects of Quaternary sediments in Poland
Autorzy:
Nowicki, Z.
Sadurski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2062975.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Quaternary aquifer
porous aquifers
regional groundwater flow systems
hydrogeology of Poland
Opis:
The major groundwater resources in Poland come from Quaternary aquifers. Rich in groundwater are structures of contemporary river valleys and of buried valleys, that comprise sands and gravels of glaciofluvial origin. Groundwater aquifers cover water demands of ca. 2.1 km3 annually. 65% of drinking water in Poland comes from groundwater intakes. Recharge zones of these aquifers are usually located in highlands – moraine plateau, and discharge zones are located in deep and wide river valleys. The average thickness of fresh water aquifers is about 200 m in Poland. The fresh water was stated even over 1,000 m depth in some places, but in the Mesozoic strata. The thickness of fresh water aquifer reduces, however, to only few metres in areas of salt water ascension or intrusion along the Baltic coast area. Recognition of groundwater circulation systems is the basis for delineation of a groundwater body (GWB). In Poland, the most productive parts of groundwater bodies that allow to abstract water at a rate grater that 10,000 m3/day, are defined as Major Groundwater Basins (MGWBs). The mean residence time of groundwater in Quaternary aquifers in Poland is estimated at some 50 yrs, whereas the residence time of water in sluggish circulation systems in deeper strata exceeds 104 yrs. Quaternary aquifers situated close to the surface area are vulnerable to municipal and agricultural pollution. The geogenic pollution such as sea water intrusion or ascension of brines are observed mainly at lowlands along the Baltic coastline, in vicinity of water intakes, or on an axial zone of anticlinoria. Trends in lowering a groundwater table are noted in the central part of the Polish lowlands and are associated with climatic variability or lignite opencast dewatering.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2010, 441 Hydrogeologia z. 10; 123--129
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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